Paris Basin

Definition and stakes

Portrait of Sir Charles Lyell Sir Charles Lyell,  A Manual of Elementary Geology

“ The newest of these, like the Faluns of the Loire, have no true representatives, or exact chronological equivalents, in the British Isles. Their place in the series will best be understood by referring to the order of superposition of the successive deposits found in the neighbourhood of Paris. The area which has been called the Paris basin is about 180 miles in its greatest length from north-east to south-west, and about 90 miles from east to west. This space may be described as a depression in the chalk, which has been filled up by alternating groups of marine and freshwater strata. ”
Source: Gutenberg

1911 Encyclopædia Britannica (1910)

“ The Paris basin is made of strata similar to those in the London and Hampshire basins. Strictly speaking, a structural basin is formed of rock beds which exhibit a centroclinal dip; an elongated narrow syncline or trough is not a basin. “Rock-basins” are comparatively small, steep-sided depressions that have been scooped out of the solid rock in mountainous regions, mainly through the agency of glaciers (see Cirque) . Lakes sometimes occupy basins that have been caused by the removal in solution of some of the more soluble constituents (rock salt, &c.) ”
Source: Wikisource

John Phillips,  A Treatise on Geology (1852)

“ The freshwater sediments of the Paris basin, studied in connection with those of Auvergne, Velay, and Cantal, offer a very complete view of the eocene lake deposits, and lead to the conclusion that the marine and freshwater strata of that basin are to be considered as marking sometimes the independent action of the sea and land floods in one basin, and sometimes their periodical alternation; the land floods always coming from the south, and the marine sediments from the north or west. ”
Source: Wikisource

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